XX 



Introduction to the Makeestoun Obseevations, 1844. 



19. The value of the absohite horizontal intensity is determined from the ob- 

 servations as follows :— If rhe the distance from the centre of the suspended magnet, 

 at which the centre of the deflecting bar is placed on the wooden beam, its axis being 

 in the line at right angles to the magnetic meridian passing through the centre of the 

 suspended magnet ; and if w be the resulting angle, through which the suspended 

 magnet is deflected, then since, by Gauss's theory, the ratio of the magnetic moment 

 m of the deflecting bai- to X, the horizontal component of the earth's magnetic force, 

 is given by the following formula 



»l 1 o . 1 



— = — r'' tan u 



X 2 1+4+4+&C. 



where /> and q are quantities depending on the mode of distribution of the magnet- 

 ism in the magnetic bars, the value of the ratio may be determined from observa- 

 tions at three distances ; it is probable, however, that the deflections are too small 

 in the observations for 1844 to render the consideration of the quantity q of import- 

 ance : the values of the ratio have in consequence been determined from observa- 

 tions at two distances ; if these be r and r', and the corresponding deflections be m 



and m', then 



»?_/' tan ti — r" tan u 



X 2 (/^-r^) 



tan M beinff obtained from the formula 



tan M=tan \- [(«i + i«-«o + o«) - /('VM-^i+^)} (1 + *)!■ -^ u~ f\ 

 L4 J y—q\}i—tv) 



where a is the angular value of one division of the long scale, / is the coeificient for 

 reducing the divisions of the short scale to the value of divisions of the long scale ; 

 ?«i and iM are the observed mean scale readings of the unifilar magnetometer, the de- 

 flecting bar, with its north pole towards the east, being at a given distance to the 

 east and west respectively of the suspended magnet; similarly, «„ and „m are the 

 mean scale readings when the deflecting bar, at the same distance, has its north pole 

 towards the west : (Zj, i(Z, &c., are the simultaneous mean scale readings of the de- 

 clinometer corresponding to Mi, it«, &c. : 1 + * is the torsion factor. [The quan- 

 tity within brackets is given for each distance, pages 166 and 167, in the column, 

 Deflection corrected for Torsion.] The last factor reduces the value of the tangent 

 to the value of X and m at the time of vibration, Ic being the coefldcient for reducing 

 the scale divisions of the bifilar magnetometer to parts of horizontal force, hd and 6„ 

 are the mean scale readings of the bifilar at the times of deflection and vibration re- 

 spectively ; q is the temperature coefiicient for the deflecting bar, t^ and t„ are the 

 mean temperatures of the bar during deflection and vibration respectively. 



The values of log \ »•' tan u are given for each distance, pages 166 and 167. 



